LAUSR

Regional climate models (RCMs) are usually initialized and driven through the boundaries of their limited area domain by data provided by global models (GCMs). The mismatch between the low‐resolution GCM initial conditions and RCM's high resolution introduces physical inconsistencies between the various components of the RCM. These inconsistencies can be resolved by running the RCM during a period that is considered unreliable: the spin‐up period. There is no deterministic definition of the length that the spin‐up period should have. Here we try to provide general guidelines that can be used to the advantage of the community. We base our analysis on Weather Research and Forecasting (WRF) simulations over a Euro‐Cordex compliant domain and find that for 2‐m temperature and precipitation, rather short spin‐up periods (1 week) can be sufficient. Nevertheless, longer periods (6 months) are advisable, and start dates in non‐winter months should be pursued, as this ensures a more realistic representation of the snow cover. Thus, the issue is not only about the spin‐up length. As the soil subsystem evolves slowly and requires longer periods to reach equilibrium than the longest considered here (1 year), seasonality plays an important role in minimizing the impact of the unreliability of the soil initialization. Fortunately, except for goals where the deep soil‐atmosphere feedback are critical, the lack of equilibrium between them can be ignored, as it seems to have little effect on the simulation of the atmospheric variables most frequently used in RCM studies.